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Journal articles on the topic 'Somma-Vesuvio'

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Author: Grafiati
Published: 10 March 2023

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1

Alberico, I., P. Petrosino, and L. Lirer. "Volcanic hazard and risk assessment in a multi-source volcanic area: the example of Napoli city (Southern Italy)." Natural Hazards and Earth System Sciences 11, no. 4 (April 7, 2011): 1057–70. http://dx.doi.org/10.5194/nhess-11-1057-2011.

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Abstract. The possible emplacement of pyroclastic fall and flow products from Campi Flegrei and Somma-Vesuvio represents a threat for the population living in Napoli city. For this area, the volcanic hazard was always partially investigated to define the hazard related to the Campi Flegrei or to the Somma-Vesuvio activity one at a time. A new volcanic hazard and risk assessment, at the municipality scale, as a vital tool for decision-making about territorial management and future planning, is presented here. In order to assess the hazard related to the explosive activity of both sources, we integrated the results of field studies and numerical simulations, to evaluate the future possibility for Napoli to be hit by the products of an explosive eruption. This is defined for the Somma Vesuvio central volcano through the sum of "field frequency" based on the thickness and distribution of past deposits (Lirer et al., 2001), and for the Campi Flegrei volcanic field by suitably processing simulated events based on numerical modelling (Alberico et al., 2002; Costa et al., 2009). Aiming at volcanic risk assessment, the hazard areas were joined with the exposure map, considered for our purposes as the economical value of artefacts exposed to hazard. We defined four risk classes, and argued that the medium and low-very low risk classes have the largest extent in Napoli municipality, whereas only few zones located in the eastern part of the city and in the westernmost coastal area show a high risk, owing to the correspondence of high economical value and high hazard.
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2

Berrino, Giovanna, Ugo Coppa, Giuseppe De Natale, and Folco Pingue. "Recent geophysical investigation at Somma-Vesuvio volcanic complex." Journal of Volcanology and Geothermal Research 58, no. 1-4 (November 1993): 239–62. http://dx.doi.org/10.1016/0377-0273(93)90111-4.

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3

Balassone, G., A. Beran, and Karl Lueger-Ring. "Variable water content of nepheline from Somma-Vesuvio, Italy." Mineralogy and Petrology 52, no. 1-2 (1995): 75–83. http://dx.doi.org/10.1007/bf01163127.

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4

Ballirano, Paolo, Adriana Maras, Peter R. Buseck, Su Wang, and Ann M. Yates. "Improved powder X-ray data for cancrinites I: Afghanite." Powder Diffraction 9, no. 1 (March 1994): 68–73. http://dx.doi.org/10.1017/s0885715600019722.

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Afghanite is a feldspathoid of the cancrinite-group: It is hexagonal, space group P63mc. The afghanite sample was found in the M. Somma-Vesuvio volcanic complex (Italy) and was previously described as davyne: Calculated cell parameters are a = 12.7997(4) Å, c = 21.4062(11) Å; the volume is 3037.2(2) Å3. The strongest lines are: 3.694(100), 3.647(56), 4.826(30), 2.678(25), 2.134(18), 3.999(12), 2.750(12), and 2.771(10). The new data provide quantitative measurement of intensities, an increased number of indexed peaks, and a different empirical formula with respect to the PDF 20-1086.
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5

Lirer, Lucio, Paola Petrosino, Ines Alberico, and Immacolata Postiglione. "Long-term volcanic hazard forecasts based on Somma-Vesuvio past eruptive activity." Bulletin of Volcanology 63, no. 1 (May 8, 2001): 45–60. http://dx.doi.org/10.1007/s004450000121.

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6

PORRECA, M., V. ACOCELLA, E. MASSIMI, M. MATTEI, R. FUNICIELLO, and A. DEBENEDETTI. "Geometric and kinematic features of the dike complex at Mt. Somma, Vesuvio (Italy)." Earth and Planetary Science Letters 245, no. 1-2 (May 15, 2006): 389–407. http://dx.doi.org/10.1016/j.epsl.2006.02.027.

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7

Donatella, De Rita, Dolfi Daniela, and Cimarelli Corrado. "Occurrence of Somma-Vesuvio fine ashes in the tephrostratigraphic record of Panarea, Aeolian Islands." Journal of Volcanology and Geothermal Research 177, no. 1 (October 2008): 197–207. http://dx.doi.org/10.1016/j.jvolgeores.2007.11.007.

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8

Caliro, S., G. Chiodini, R. Avino, C. Cardellini, and F. Frondini. "Volcanic degassing at Somma–Vesuvio (Italy) inferred by chemical and isotopic signatures of groundwater." Applied Geochemistry 20, no. 6 (June 2005): 1060–76. http://dx.doi.org/10.1016/j.apgeochem.2005.02.002.

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9

Chukanov, Nikita V., Natalia V. Zubkova, Igor V. Pekov, Lyudmila V. Olysych, Elena Bonaccorsi, and Dmitry YU Pushcharovsky. "Balliranoite, (Na,K)6Ca2(Si6Al6O24)Cl2(CO3), a new cancrinite-group mineral from Monte Somma Vesuvio volcanic complex, Italy." European Journal of Mineralogy 22, no. 1 (March 18, 2010): 113–19. http://dx.doi.org/10.1127/0935-1221/2010/0022-1983.

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10

Rolandi, G., S. Maraffi, P. Petrosino, and L. Lirer. "The Ottaviano eruption of Somma-Vesuvio (8000 y B.P.): a magmatic alternating fall and flow-forming eruption." Journal of Volcanology and Geothermal Research 58, no. 1-4 (November 1993): 43–65. http://dx.doi.org/10.1016/0377-0273(93)90101-v.

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11

Tadini, A., M. Bisson, A. Neri, R. Cioni, A. Bevilacqua, and W. P. Aspinall. "Assessing future vent opening locations at the Somma-Vesuvio volcanic complex: 1. A new information geodatabase with uncertainty characterizations." Journal of Geophysical Research: Solid Earth 122, no. 6 (June 2017): 4336–56. http://dx.doi.org/10.1002/2016jb013858.

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12

Rispoli, Concetta, Renata Esposito, Luigi Guerriero, and Piergiulio Cappelletti. "Ancient Roman Mortars from Villa del Capo di Sorrento: A Multi-Analytical Approach to Define Microstructural and Compositional Features." Minerals 11, no. 5 (April 29, 2021): 469. http://dx.doi.org/10.3390/min11050469.

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This research provides a characterization of ancient Roman mortars from “Villa del Capo di Sorrento” (commonly known as “Villa di Pollio Felice” or “Bagni della Regina Giovanna”). A deepened analysis of cementitious binding matrix and aggregates was conducted with the aims of determining possible sources of raw materials and the mix recipe, and to evaluate the minerogenetic secondary processes. Twenty samples taken from the Villa were investigated by means of a multi-analytical approach, including polarized optical microscopy on thin sections, X-ray powder diffraction, scanning electron microscopy analysis, energy dispersed spectrometry, simultaneous thermal analyses, and mercury intrusion porosimetry. Bedding mortars were made with slaked lime mixed with volcanic materials, whereas coating mortars were made adding to previous recipe as ceramic fragments. All samples were classified as hydraulic mortars. Cementitious binding matrix was characterized by gel-like C-A-S-H, calcite, hydrocalumite, and gypsum, deriving from lime/pozzolanic material. Geomaterials used for mortar production had a local origin. Pozzolanic materials, such as volcanic fragments, scoriae, pumice, and crystal fragments derived from both pyroclastic rocks of the Campi Flegrei district and from rocks of the Somma-Vesuvio complex; porosity test suggest that the products related to minerogenetic secondary processes, make mortars more resistant.
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13

Tadini, A., A. Bevilacqua, A. Neri, R. Cioni, W. P. Aspinall, M. Bisson, R. Isaia, et al. "Assessing future vent opening locations at the Somma-Vesuvio volcanic complex: 2. Probability maps of the caldera for a future Plinian/sub-Plinian event with uncertainty quantification." Journal of Geophysical Research: Solid Earth 122, no. 6 (June 2017): 4357–76. http://dx.doi.org/10.1002/2016jb013860.

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14

Tullio Ricci, Rosa Nave, and Franco Barberi. "Vesuvio civil protection exercise MESIMEX: survey on volcanic risk perception." Annals of Geophysics 56, no. 4 (November 11, 2013). http://dx.doi.org/10.4401/ag-6458.

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<p>In October 2006 the European Civil Protection Exercise MESIMEX (Somma Vesuvio Mesimex – Major Emergency SIMulation Exercise) on volcanic risk took place at Vesuvio, promoted by Campania Region and coordinated by the Italian Civil Protection Department. The exercise was focused on the preparedness phase for a major volcanic emergency in the area of Vesuvio. An evacuation of a sample of 1800 inhabitants from the Vesuvio Red Zone was also tested during the drill because the emergency plan ensures the complete evacuation of the population from the higher risk zone before the onset of the eruption. During that event a survey on volcanic risk perception was carried out on the evacuated population in order to compare the results with the ones coming from a previous similar survey, using the same questionnaire, carried out on a wider sample of residents in the Vesuvio Red Zone few months before MESIMEX exercise. The aim was to point out any differences in population’s attitude towards volcanic risk after having received detailed information on the emergency plan and on the hazards and risk related to the reactivation of Vesuvio, and experiencing the exercise. 463 questionnaires were distributed to the population evacuated from the 18 municipalities of the Red Zone and participating to the exercise. Main results in comparing data from MESIMEX survey with the Vesuvio previous one, put in evidence how the general level of Vesuvio residents’ trust remains quite low, indicating that a continuous and effective effort has to be done by both scientific community and Civil Protection Department. Particular attention should be paid in education and outreach activities and in involving people in risk mitigation procedures, also through more frequent exercises.</p>
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15

Umberto Tammaro, Prospero De Martino, Francesco Obrizzo, Giuseppe Brandi, Andrea D’Alessandro, Mario Dolce, Santa Malaspina, Claudio Serio, and Folco Pingue. "Somma Vesuvius volcano: ground deformations from CGPS observations (2001-2012)." Annals of Geophysics 56, no. 4 (November 12, 2013). http://dx.doi.org/10.4401/ag-6462.

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<p>This paper is a contribution to the evaluation of ground deformations at Somma-Vesuvius volcano by means GPS measurements from 2001 to 2012. In this study we use a dataset from nine continuous GPS stations of the Neapolitan Volcanoes Continuous GPS network (NeVoCGPS), which covers the Neapolitan volcanic area, and is operated by the Istituto Nazionale di Geofisica e Vulcanologia. The GPS data processing is performed by the Bernese software v. 5.0. The results of the data processing show that the dynamics of the Somma-Vesuvio volcano, between 2001 and 2012, is characterized by a general subsidence, with maximum values on the Gran Cono at BKNO (−11.7 ± 0.65 mm/year) and BKE1 (−4.92 ± 0.36 mm/year) stations. The subsidence decrease from the crater down to the coast and the horizontal displacements are concentrated in Gran Cono area, the youngest part of the volcano. The parameters of the principal strain components indicate that Somma-Vesuvius is affected by a predominant contraction phase, which is concentrated in the areas with the greatest altitudes.</p>
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16

Acocella, V., M. Porreca, M. Neri, E. Massimi, and M. Mattei. "Propagation of dikes at Vesuvio (Italy) and the effect of Mt. Somma." Geophysical Research Letters 33, no. 8 (2006). http://dx.doi.org/10.1029/2005gl025590.

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